Anthropogenic carbon distributions in the Atlantic Ocean: data-based estimates from the Arctic to the Antarctic
Type | Article | ||||||||||||
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Date | 2009-03-18 | ||||||||||||
Language | English | ||||||||||||
Author(s) | Vazquez-Rodriguez Marcos1, Touratier Franck2, Lo Monaco Claire3, Waugh D. W.4, Padin X. A.1, Bellerby R. G. J.5, 6, Goyet Catherine2, Metzl Nicolas3, Rios Aida F.1, Perez Fiz F.1 | ||||||||||||
Affiliation(s) | 1 : CSIC, Inst Invest Marinas, Vigo 36208, Spain. 2 : Univ Perpignan, IMAGES, F-66860 Perpignan, France. 3 : Univ Paris 06, LOCEAN IPSL, F-75252 Paris 05, France. 4 : Johns Hopkins Univ, Dept Earth & Planetary Sci, Baltimore, MD 21218 USA. 5 : Univ Bergen, Bjerknes Ctr Climate Res, N-5007 Bergen, Norway. 6 : Univ Bergen, Inst Geophys, N-5007 Bergen, Norway. |
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Source | Biogeosciences (1726-4170) (Copernicus Gesellschaft Mbh), 2009-03-18 , Vol. 6 , N. 3 , P. 439-451 | ||||||||||||
DOI | 10.5194/bg-6-439-2009 | ||||||||||||
WOS© Times Cited | 98 | ||||||||||||
Keyword(s) | deep equatorial atlantic, northern indian-ocean, water mass ages, CO2, sea, transport, increase, tracers, models | ||||||||||||
Abstract | Five of the most recent observational methods to estimate anthropogenic CO2 (C-ant) are applied to a high-quality dataset from five representative sections of the Atlantic Ocean extending from the Arctic to the Antarctic. Between latitudes 60 degrees N-40 degrees S all methods give similar spatial distributions and magnitude of C-ant. However, discrepancies are found in some regions, in particular in the Southern Ocean and Nordic Seas. The differences in the Southern Ocean have a significant impact on the anthropogenic carbon inventories. The calculated total inventories of C-ant for the Atlantic referred to 1994 vary from 48 to 67 Pg (10(15) g) of carbon, with an average of 54 +/- 8 Pg C, which is higher than previous estimates. These results, both the detailed C-ant distributions and extrapolated inventories, will help to evaluate biogeochemical ocean models and coupled climate-carbon models. | ||||||||||||
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